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在高光谱数据模式分解方法(PDM)的基础上,建立了一种新的植被指数(VIPD)。根据地面植被光合成实验,建立了有效光合成曲线植被净初级生产力(NPP)遥感估算模型,利用2001年各月份的MODIS影像数据,估算得到纪伊半岛地区的各类NPP。研究发现,该地区的温带常绿林NPP年均值与2001年IPCC调查报告和地面实测得到的估算值在误差范围内一致。实验证明,该光合成曲线NPP估算模型能够有效地利用高光谱数据,且能较好地应用于温带植被研究。 相似文献
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基于环境星CCD数据的冬小麦叶面积指数遥感监测模型研究 总被引：11，自引：0，他引：11
以山东禹城为研究区,利用我国自主研发的环境星数据,计算了4种植被指数,即归一化植被指数(NDVI)、比值植被指数(RVI)、土壤调节植被指数(SAVI)及增强型植被指数(EVI);结合同步观测数据,将植被指数与实测叶面积指数(LAI)进行回归分析,比较各种植被指数模型对冬小麦LAI的估测精度。结果表明,4种植被指数与LAI均具有较高的相关性,其中,比值植被指数(RVI)对LAI反演精度最高,即LAI=2.967 lnRVI-1.201是估算冬小麦LAI的最优模型。使用2009年5月冬小麦LAI观测数据对模型进行验证,平均相对误差为19%。 相似文献
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基于GIS、RS的黄土高原USLE模型改进方法 总被引：2，自引：0，他引：2
结合地理信息系统技术、遥感技术，探讨美国通用土壤流失方程（USLE）在我国黄土高原土壤侵蚀产沙模型应用中的改进方法。USLE属于因子分析模型，由于USLE考虑因素全面，因子具有物理意义，形式简单，所用资料广泛，统一了土壤侵蚀模型形式，故在全世界得到了广泛应用。但是我国黄土高原地区土壤流失严重，影响流失的因素极其多样，使得USLE模型不能很好的应用于该地特殊的地理条件。基于此，采用GIS方法探讨USLE模型在黄土高原改进方法问题。 相似文献
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基于MODIS的植被指数变化研究及其与气候因子的关系分析 总被引：1，自引：0，他引：1
以2012年1~12月的MODIS 13Q1数据产品为基础,提取四川西南地区7市植被指数进行相关分析。基于各月植被指数,采用对比分析法,研究植被指数时空变化规律。同时,结合研究区内2012年月降水量和气温月平均值,选择多项式拟合法,对EVI,NDVI月平均值进行相关性分析,研究植被指数与气候因子的相关性。 相似文献
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通过对比分析MODIS数据的标准归一化差分植被指数、土壤调节植被指数及增强型植被指数的特点,最终选择标准归一化差分植被指数(NDVI)对工程区进行监测。并阐述了最大合成法合成MODIS植被指数是一种行之有效的方法。 相似文献
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冬小麦叶面积指数的高光谱估算模型研究 总被引：2，自引：0，他引：2
本文以山东禹城为研究区,利用地面实测光谱数据,探讨不同植被指数和红边参数建立高光谱模型反演冬小麦叶面积指数的精度。通过逐波段分析计算了4种植被指数(NDVI、RVI、SAVI、EVI),结合同步观测LAI数据,确定反演叶面积指数的最优波段;计算了5种常用的高光谱植被指数MCARI、MCARI2、OSAVI、MTVI2、MSAVI2,同时利用4种常用方法计算红边位置和红谷,与实测LAI进行回归分析,比较植被指数和红边参数模型对冬小麦LAI的估测精度。结果表明各因子与LAI均具有较高的相关性,整个研究区归一化植被指数具有最高的反演精度,确定了估算冬小麦LAI的最优模型,并使用独立的LAI观测数据对模型进行了验证。 相似文献
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基于冠层反射光谱的水稻产量预测模型 总被引：21，自引：0，他引：21
基于地面实测的水稻冠层反射光谱,计算了常用的8个植被指数,并在产量形成生理特征的基础上,系统分析了水稻籽粒产量及其构成因素与各植被指数之间的关系。结果表明,通过单一生育时期或某个生育阶段的光谱植被指数来直接估测产量精度较低。发现叶面积氮指数(叶片氮百分含量与叶面积指数的乘积)的变化趋势很好地反映了产量的形成过程,且与光谱植被指数极显著正相关,基于此建立了水稻的光谱植被指数-累积叶面积氮指数-产量估测模型(VICLANIYieldModel)。并将其与LAD-产量模型、多生育期复合估产模型进行了比较,表明本模型预测精度最高。 相似文献
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为准确提取水稻面积,以东北为研究区域,采用多时相16d合成MODIS增强型植被指数数据和8d合成MODIS地表反射率数据提取水稻种植分布。选取水稻代表样点利用IDL编程提取物候曲线,利用归一化植被指数(NDVI)将水稻与其他明显地类区分,然后建立水稻增强型植被指数(EVI)、地表水体指数(LSWI)之间的相关关系,结合最新2015年土地利用数据提取东北三省2015年水稻种植面积。同时运用运筹学理论建立省级尺度水稻判别条件最优化模型,分析其在空间分布上的差异性和相关性,并将结果与统计年鉴进行对比分析,分析表明MODIS数据适合大区域省级范围水稻面积的提取,精度可达90%以上。由此得出,MODIS数据在省级尺度提取水稻种植面积上有着较大的优势。 相似文献
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基于MODIS影像的山西省植被指数分析 总被引：2，自引：0，他引：2
以MODIS遥感影像为数据源,利用ENVI遥感影像处理软件,笔者对山西省2005年9月和2006年9月两期MODIS影像的植被指数进行计算,建立了两期植被指数密度分割模型,以获得全省植被覆盖的整体状况,通过对两期植被指数影像图进行动态链接、叠加以及结合相减比较,可以看出两年间全省的植被覆盖空间变化情况。结果表明:全省较低植被覆盖区不多,高植被地区主要分布在中部以南地区,中低植被覆盖集中在中部以北地区。两年的植被指数比较结果表明,全省中等植被覆盖区有所增加,但高植被覆盖区增加不明显。 相似文献
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长江上游小流域土壤侵蚀动态模拟与分析 总被引：1，自引：0，他引：1
以长江上游甘肃省尚沟流域为研究区,在遥感影像和GIS空间分析技术支撑下,根据USLE因子算法生成各因子栅格图,借助地图代数运算,估算了尚沟流域1998年和2004年的土壤侵蚀量,并对2004年土壤侵蚀与其环境背景因子进行叠加和空间统计分析。在此基础上,构建了与GIS软件平台集成的地理元胞自动机,模拟了该流域2004年、2010年和2020年土壤侵蚀空间演化情形。结果表明:研究区平均侵蚀量从1998年的6598.1t/km2下降到2004年的5923.3t/km2,侵蚀面积净减少172.3hm2,输沙量减少9.15×104t;1300～1400m的海拔高程带、25～35°坡度带、南坡和旱耕地是发生水土流失的主要区域;经模拟,2010年总侵蚀面积为93.49km2,侵蚀总量73.15×104t,侵蚀模数为5126t/km2,土壤侵蚀状况总体上将有所减缓。 相似文献
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K. Meusburger N. KonzM. Schaub C. Alewell 《International Journal of Applied Earth Observation and Geoinformation》2010
The focus of soil erosion research in the Alps has been in two categories: (i) on-site measurements, which are rather small scale point measurements on selected plots often constrained to irrigation experiments or (ii) off-site quantification of sediment delivery at the outlet of the catchment. Results of both categories pointed towards the importance of an intact vegetation cover to prevent soil loss. With the recent availability of high-resolution satellites such as IKONOS and QuickBird options for detecting and monitoring vegetation parameters in heterogeneous terrain have increased. The aim of this study is to evaluate the usefulness of QuickBird derived vegetation parameters in soil erosion models for alpine sites by comparison to Cesium-137 (Cs-137) derived soil erosion estimates. The study site (67 km2) is located in the Central Swiss Alps (Urseren Valley) and is characterised by scarce forest cover and strong anthropogenic influences due to grassland farming for centuries. A fractional vegetation cover (FVC) map for grassland and detailed land-cover maps are available from linear spectral unmixing and supervised classification of QuickBird imagery. The maps were introduced to the Pan-European Soil Erosion Risk Assessment (PESERA) model as well as to the Universal Soil Loss Equation (USLE). Regarding the latter model, the FVC was indirectly incorporated by adapting the C factor. Both models show an increase in absolute soil erosion values when FVC is considered. In contrast to USLE and the Cs-137 soil erosion rates, PESERA estimates are low. For the USLE model also the spatial patterns improved and showed “hotspots” of high erosion of up to 16 t ha−1 a−1. In conclusion field measurements of Cs-137 confirmed the improvement of soil erosion estimates using the satellite-derived vegetation data. 相似文献
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The quantitative assessment of spatial soil erosion is valuable information to control the erosion. The study area in a part of Narmada river in central India is selected. The main objective is to assess and compare the results obtained from three soil erosion models using GIS platform. Variation in the rate of erosion of the three models is compared considering varying slope, soil and land use of the area. Three models selected are Morgan–Morgan–Finney (MMF), Universal Soil Loss Equation (USLE) and Revised Universal Soil Loss Equation (RUSLE). The best fit or the most reliable model for the study area is selected after validation with the observed sedimentation data. The results give –39.45%, –9.60% and 4.80% difference in the values of sedimentation by MMF, USLE and RUSLE, respectively, from the observed data. Finally, RUSLE model has been found to be most reliable for the study area. 相似文献
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Quantitative Determination of Soil Erosion and Prioritization of Micro-Watersheds Using Remote Sensing and GIS 总被引：5，自引：0，他引：5
Vipul Shinde Arabinda Sharma Kamlesh N. Tiwari Manjushree Singh 《Journal of the Indian Society of Remote Sensing》2011,39(2):181-192
Soil erosion which occurs at spatially varying rate is a widespread threat to sustainable resource management at watershed scale. Thus estimation of soil loss and identification of critical area for implementation of best management practice is central to success of soil conservation programme. The present study focuses application of most widely used Universal Soil Loss Equation (USLE) to determine soil erosion and prioritization of micro-watersheds of Upper Damodar Valley Catchment (UDVC) of India. Annual average soil loss for the entire basin is 23.17 t/ha/yr; for micro-watersheds. High soil loss is observed in 345 micro-watersheds, medium in 159 micro-watersheds and low soil loss is observed in 201 micro-watersheds. It is found that, out of 705 micro-watersheds of UDVC, 453 micro-watersheds are in agreement with AISLUS suggested priority which is based on observed sediment yield, 116 micro-watersheds under predict and 136 micro-watersheds over predict the priority. Geographic Information System (GIS) is applied to prepare various layers of USLE parameters which interactively estimate soil erosion at micro-watershed level. The main advantage of the GIS methodology is in providing quick information on the estimated value of soil loss for any part of the investigated area. 相似文献
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Soil erosion prediction based on land cover dynamics at the Semenyih watershed in Malaysia using LTM and USLE models 总被引：1，自引：0，他引：1
This study attempts to identify and forecast future land cover (LC) by using the Land Transformation Model (LTM), which considers pixel changes in the past and makes predictions using influential spatial features. LTM applies the Artificial Neural Networks algorithm) in conducting the analysis. In line with these objectives, two satellite images (Spot 5 acquired in 2004 and 2010) were classified using the Maximum Likelihood method for the change detection analysis. Consequently, LC maps from 2004 to 2010 with six classes (forest, agriculture, oil palm cultivations, open area, urban, and water bodies) were generated from the test area. A prediction was made on the actual soil erosion and the soil erosion rate using the Universal Soil Loss Equation (USLE) combined with remote sensing and GIS in the Semenyih watershed for 2004 and 2010 and projected to 2016. Actual and potential soil erosion maps from 2004 to 2010 and projected to 2016 were eventually generated. The results of the LC change detections indicated that three major changes were predicted from 2004 to 2016 (a period of 12 years): (1) forest cover and open area significantly decreased at rates of almost 30 and 8 km2, respectively; (2) cultivated land and oil palm have shown an increment in sizes at rates of 25.02 and 5.77 km2, respectively; and, (3) settlement and Urbanization has intensified also by almost 5 km2. Soil erosion risk analysis results also showed that the Semenyih basin exhibited an average annual soil erosion between 143.35 ton ha?1 year?1 in 2004 and 151 in 2010, followed by the expected 162.24 ton ha?1 year?1. These results indicated that Semenyih is prone to water erosion by 2016. The wide range of erosion classes were estimated at a very low level (0–1 t/ha/year) and mainly located on steep lands and forest areas. This study has shown that using both LTM and USLE in combination with remote sensing and GIS is a suitable method for forecasting LC and accurately measuring the amount of soil losses in the future. 相似文献
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Javed Mallick Yasser Alashker Shams Al-Deen Mohammad Mohd Ahmed Mohd Abul Hasan 《国际地球制图》2013,28(8):915-940
Soil erosion is the most important factor in land degradation and influences desertification in semi-arid areas. A comprehensive methodology that integrates revised universal soil loss equation (RUSLE) model and GIS was adopted to determine the soil erosion risk (SER) in semi-arid Aseer region, Saudi Arabia. Geoenvironmental factors viz. rainfall (R), soil erodibility (K), slope (LS), cover management and practice factors were computed to determine their effects on average annual soil loss. The high potential soil erosion, resulting from high denuded slope, devoid of vegetation cover and high intensity rainfall, is located towards the north western part of the study area. The analysis is investigated that the SER over the vegetation cover including dense vegetation, sparse vegetation and bushes increases with the higher altitude and higher slope angle. The erosion maps generated with RUSLE integrated with GIS can serve as effective inputs in deriving strategies for land planning/management in the environmentally sensitive mountainous areas. 相似文献
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Mushtak Jabbar 《地球空间信息科学学报》2013,16(1):34-37
This paper describes the use of the Arc/Info and ArcView GIS tools to estimate soil erosion with Universal Soil Loss Equation (USLE). Calculations are be done by using capabilities available. This study start with a digital elevation model (DEM) of Shaanxi, which was created by digitizing contour and spot heights from the topographic map on 1∶250 000 scale and grid themes for the USLEK andC factors. It is note worthy that USLEK can be obtained by adding the K factor as an attribute to a soil theme's table. TheC can be obtained from tables or using the information about land use and management given by USLE program. A land use theme can be used to add theC factors as an attribute field. The purpose of this study is to establish spatial information of soil erosion using USLE and GIS and discuss the analysis of the soil erosion and slope failures in GIS and formulate the possible framework. 相似文献
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Moderate Resolution Imaging Spectroradiometer (MODIS) 16-day 1-km vegetation index products, daily temperature, photosynthetically active radiation (PAR), and precipitation from 2001 to 2004 were utilized to analyze the temporal variations of the MODIS normalized difference vegetation index (NDVI) and enhanced vegetation index (EVI), as well as their correlations with climate over the evergreen forested sites in Zhejiang-a humid subtropical region in the southeast of China. The results showed that both NDVI and EVI could discern the seasonal variation of the evergreen forests. Attributed to the sufficient precipitation in the study area, the growth of vegetation is mainly controlled by energy; as a result, NDVI, and especially EVI, is more correlated with temperature and PAR than precipitation. Compared with NDVI, EVI is more sensitive to climate condition and is a better indicator to study vegetation variations in the study region 相似文献